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On the production of N(+) by energetic electronsCalculations of the ratio of N(+) to total N2 ion production for auroral electrons which give a value of 0.16 compared to the value of 0.22 that has been assumed in a recent publication is presented. The corresponding ratio for photoelectron production is 0.05, which makes photoelectron production of N(+) negligible compared to photodissociative production. The ratio of 3914-A to total ion production is found to be 0.07 for auroral electrons and a similar 0.06 for photoelectrons. The 3371-A ratio to total N2 ion production is 0.09. This calculation also reveals that the secondary electrons in auroras, with energies less than 100 eV, produce only about one third of the total number of ions produced. Only one quarter of the N(+) ions are created by secondary electrons.
Document ID
19860025608
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Richards, P. G.
(Utah State Univ. Logan, UT, United States)
Torr, D. G.
(Utah State University Logan, United States)
Date Acquired
August 12, 2013
Publication Date
October 1, 1985
Publication Information
Publication: Journal of Geophysical Research
Volume: 90
ISSN: 0148-0227
Subject Category
Geophysics
Accession Number
86A10346
Funding Number(s)
CONTRACT_GRANT: NSF ATM-82-19712
CONTRACT_GRANT: NAGW-406
CONTRACT_GRANT: NSF ATM-83-12633
CONTRACT_GRANT: NAGW-105
CONTRACT_GRANT: NSF ATM-84-17843
CONTRACT_GRANT: NSF ATM-84-15675
Distribution Limits
Public
Copyright
Other

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